Preprints
https://doi.org/10.5194/egusphere-2024-2018
https://doi.org/10.5194/egusphere-2024-2018
05 Jul 2024
 | 05 Jul 2024

Lagrangian characterization of heat waves: The perspective matters

Amelie Mayer and Volkmar Wirth

Abstract. Although heat waves are one of the most dangerous types of weather-related hazards, their underlying mechanisms are not yet sufficiently understood. Especially, there is still no scientific consensus about the relative importance of the three key processes: horizontal temperature transport, subsidence accompanied by adiabatic heating, and diabatic heating. The current study quantifies these processes using a Eulerian method based on tracer advection, which allows one to extract Lagrangian information. For each grid point at any time, the method yields a decomposition of temperature anomalies into the aforementioned processes, complemented by the contribution of a pre-existing anomaly. Two different approaches for this decomposition are employed. The first approach is based on full (absolute) fields of the respective terms, whereas the second approach is based on anomaly fields of the respective terms, i.e., deviations from their corresponding climatologies. The two approaches offer two distinct perspectives on the same subject matter. By analyzing two recent heat waves, it is shown that the two decompositions yield substantial differences regarding the relative importance of the processes. A statistical analysis indicates that these differences are not coincidental, but characteristic for the respective regions. It is concluded that the Lagrangian characterization of heat waves is a matter of perspective.

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Journal article(s) based on this preprint

29 Jan 2025
Two different perspectives on heatwaves within the Lagrangian framework
Amelie Mayer and Volkmar Wirth
Weather Clim. Dynam., 6, 131–150, https://doi.org/10.5194/wcd-6-131-2025,https://doi.org/10.5194/wcd-6-131-2025, 2025
Short summary
Amelie Mayer and Volkmar Wirth

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2018', Anonymous Referee #1, 15 Aug 2024
  • RC2: 'Comment on egusphere-2024-2018', Anonymous Referee #2, 09 Sep 2024
  • AC1: 'Comment on egusphere-2024-2018', Amelie Mayer, 08 Oct 2024

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2018', Anonymous Referee #1, 15 Aug 2024
  • RC2: 'Comment on egusphere-2024-2018', Anonymous Referee #2, 09 Sep 2024
  • AC1: 'Comment on egusphere-2024-2018', Amelie Mayer, 08 Oct 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Amelie Mayer on behalf of the Authors (08 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (18 Oct 2024) by Gwendal Rivière
RR by Anonymous Referee #2 (22 Oct 2024)
ED: Publish subject to technical corrections (15 Nov 2024) by Gwendal Rivière
AR by Amelie Mayer on behalf of the Authors (21 Nov 2024)  Author's response   Manuscript 

Journal article(s) based on this preprint

29 Jan 2025
Two different perspectives on heatwaves within the Lagrangian framework
Amelie Mayer and Volkmar Wirth
Weather Clim. Dynam., 6, 131–150, https://doi.org/10.5194/wcd-6-131-2025,https://doi.org/10.5194/wcd-6-131-2025, 2025
Short summary
Amelie Mayer and Volkmar Wirth
Amelie Mayer and Volkmar Wirth

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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.

Short summary
Although heatwaves are among the most dangerous weather-related hazards, their underlying mechanisms are not fully understood. Here, we investigate the formation of heat waves in an air-parcel based framework and distinguish the contributions from horizontal transport, vertical transport, and diabatic heating. We show that the obtained results depend profoundly on whether one compares the absolute contributions of the individual terms or, instead, their anomalies relative to climatology.